The evaluation of apparent rotations asociated with different geological structures is an important task that has to be taken into account to correctly interprete paleomagnetic data. In this paper, the way to calculate ...

This paper presents the first magnetotectonic data of the central fringe of the Jaca-Pamplona Basin. These data have been obtained from 16 sites located in marls, tirbidites and limestones of Eocene age. In the central and ...

Geometric and kinematic analysis of Pyrenean folds, cleavage and thrusts is carried out in several exceptional
outcrops of the Eocene flysch at Isaba (Navarra, Spain). Distribution, orientation and cross-cut relationshi ...

An extension of Cooper's (1983) method allows the calculation o f the bulk strain in rotated areas, If the maximum rotation of an area is known it is possible to determine the extreme values of bulk shortening for a specific ...

In the western part of the Sierras Exteriores Aragonesas the southern Pyrenean front is not a southvergent large thrust, but an isoclinal detachment fold (Santo Domingo anticline), whose core is occuppied by the Upper ...

The structure of the eastern extreme of the Jaca Basin is defined by the Gavarnie, Guara-Gèdre and Guarga
thrust sheets. The Guara-Gèdre thrust was active during mid Luttetian-earliest Chattian and the Gavarnie
thrust, ...

Based on structural, stratigraphic and gravimetric data, a regional scale N 020-040 E blind-fault, named
the Oroz-Betelu- Unzue fault, extending from the western part of the Oroz-Betelu massif to the Sierra de
Alaiz ...

The evaluation of apparent rotations asociated with different geological structures is an important task that has to be taken into account to correctly interprete paleomagnetic data. In this paper, the way to calculate ...

This paper presents the first magnetotectonic data of the central fringe of the Jaca-Pamplona Basin. These data have been obtained from 16 sites located in marls, tirbidites and limestones of Eocene age. In the central and ...

Geometric and kinematic analysis of Pyrenean folds, cleavage and thrusts is carried out in several exceptional
outcrops of the Eocene flysch at Isaba (Navarra, Spain). Distribution, orientation and cross-cut relationshi ...

An extension of Cooper's (1983) method allows the calculation o f the bulk strain in rotated areas, If the maximum rotation of an area is known it is possible to determine the extreme values of bulk shortening for a specific ...

In the western part of the Sierras Exteriores Aragonesas the southern Pyrenean front is not a southvergent large thrust, but an isoclinal detachment fold (Santo Domingo anticline), whose core is occuppied by the Upper ...

The structure of the eastern extreme of the Jaca Basin is defined by the Gavarnie, Guara-Gèdre and Guarga
thrust sheets. The Guara-Gèdre thrust was active during mid Luttetian-earliest Chattian and the Gavarnie
thrust, ...

Based on structural, stratigraphic and gravimetric data, a regional scale N 020-040 E blind-fault, named
the Oroz-Betelu- Unzue fault, extending from the western part of the Oroz-Betelu massif to the Sierra de
Alaiz ...